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Needs for Future Planetary Work

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2001 Mars Odyssey - Observed dd and streaks in THEMIS VIS and ... 2003- Mars Express - High Resolution Stereo Color (HRSC) imager. [ Stanzel et al., workshop] ... – PowerPoint PPT presentation

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Title: Needs for Future Planetary Work


1
Discussion Needs for Future Planetary
Work Working Group Bruce Cantor Fred
Calef Stephen Cumming Casey
Donohue Shane Thompson Patrick Whelley
Christina Stanzal Chris Ashburn Nathan
Drake
2
  • HISTORY of MARTIAN
    DUST DEVILS
  • 1976-1978 - Dust devils were first detected by
    the Viking Lander 1 and 2 onboard
    meteorological experiments. Ryan and Lucich,
    1983
  • This was followed by visual detection of large
    dust devils by the two Viking Orbiters, during
    northern summer. Thomas and Gierasch, 1985
  • Dust Devil Tracks observed in Viking Orbiter
    Images Grant and Schultz, 1987
  • 1997- Mars Pathfinder detects dust devils with
    the meteorological (MET) package.
  • Schoefield et al., 1997, and later
    Renno et al, 2000
  • Visual detection of dust devils at Pathfinder
    site were made with Imager for Mars Pathfinder
    (IMP) experiment. Metzger et al., 1999, 2000.
  • DDs peak activity is 1300 LST Murphy and
    Nelli, 2002
  • 1999 - Mars Global Surveyor were detected in MOC
    images. Malin and Edgett, 2001.
  • Additional studies have found more dust devils
    and tracks. Biener et al., 2002 Cantor and
    Edgett, 2002 Balme et al, 2003 Greeley et al,
    2003 Leovy, 2003 Fisher et al., 2005 Whelley,
    workshop Drake, workshop Cantor et al.,
    workshop, 2005 in preparation
  • 2001 Mars Odyssey - Observed dd and streaks in
    THEMIS VIS and later IR observations. Others
    Cushing et al, workshop, 2005 in press
  • 2003- Mars Express - High Resolution Stereo Color
    (HRSC) imager. Stanzel et al., workshop
  • 2003 - Mars Exploration Rover (MER) Spirit
    observed dd and streaks in Gusev. Greeley et
    al., 2003, 2005 Castano, workshop
    Foley,workshop
  • -DDs peak around 1100 LST, observations suggest
    small ones play no role in sustaining background
    haze. Thompson,workshop

3
Work That Needs to Be Done (1 of 2)
  • What is the true spatial and temporal
    distribution of dust devils across all of Mars?
  • What is their size distribution?
  • What are the meterological conditions associated
    with dust devils?
  • What are the wind speeds (rotational and
    vertical) and temperature profiles associated
    with martian dust devils?
  • What are the surface wind stresses needed to lift
    dust?
  • What is the size distribution of of dust being
    lifted?
  • How high is the dust being lifted?

4
Work That Needs to Be Done (2 of 2)
  • Engineering data of surface missions need to be
    at looked?
  • What is the difference between light and dark
    tone streaks? What are their seasonal and spatial
    distribution?
  • What is the role of (small and large) dust devils
    in sustaining the background opacity?
  • What are the magnet/electrostatic field
    properties of martian dust devils?
  • Determine the hazards of dust devils to surface
    and manned missions?

5
Future Platform Instruments (1 of 2)
  • How can MRO, Phoenix, MSL, (MSR?) be used to help
    address any of the outstanding questions or not?
    Is there a case for MGS, ODY, MER extension
    because of these needs?
  • - Yes, need to understand the hazards of landers
    and future manned missions, the climate, and
    weather on Mars. They can help quantify the
    spatial and temporal distribution of dust devils
    at select locations and globally.
  • How important are these needs in the big scheme
    of Mars meteorology and climate?
  • - They play some role in sustaining the
    background opacity. Need to find out what the
    magnitude of that role is.

6
Future Platform Instruments (2 of 2)
  • What are our future instrument needs based on the
    biases in the MGS, ODY, and MEX, Pathfinder and
    MER data sets?
  • - Multi-spectral visual thermal imagers,
    lidar, magnatometer, repeat coverage, higher
    altitude wind speed measurements,
    multi-simultaneous meteorological measurements
    temperature, pressure, pressure, wind shear
    stresses at the surface, just above the surface
    and slight higher, sample return, MORE
    meteorological ground stations! Possibly even a
    mini-wind tunnel on the surface of Mars.
  • What kind of payload platforms are needed?
  • - Balloons, airplanes, rovers, orbiters,
    landers, micro-machines, ect
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